Disko Island

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Disko Island
Native name:
Qeqertarsuaq
Qeqertarsuaq.JPG
Qeqertarsuaq town on Disko Island
Disko Island
Map of Disko Island
Greenland edcp location map.svg
Red pog.svg
Disko Island
Location of Disko Island in Greenland
Geography
Location Baffin Bay
Coordinates 69°45′N53°30′W / 69.750°N 53.500°W / 69.750; -53.500
Area8,578 km2 (3,312 sq mi)
Area rank 84th largest in world
2nd largest in Greenland
Length160 km (99 mi)
Highest elevation1,919 m (6296 ft)
Highest pointPyramiden
Administration
Municipality Qeqertalik
Largest settlement Qeqertarsuaq (pop. 839)
Demographics
Population1,100
Pop. density0.13/km2 (0.34/sq mi)
Ethnic groups Inuit

Disko Island (Greenlandic : Qeqertarsuaq, Danish : Diskoøen) is a large island in Baffin Bay, off the west coast of Greenland. It has an area of 8,578 km2 (3,312 sq mi), [1] making it the second largest island of Greenland after the main island and one of the 100 largest islands in the world.

Contents

Etymology

The island's Greenlandic name Qeqertarsuaq means The Large Island (from qeqertaq = island).

Geography

Flying above Disko Island in December Disko Island, Greenland in December.jpg
Flying above Disko Island in December

The island has a length of about 160 km (100 mi), rising to an average height of 975 m (3,199 ft), peaking at 1,919 m (6,296 ft). The port of Qeqertarsuaq (named after the island, and also known as Godhavn) lies on its southern coast. Blæsedalen valley is north of Qeqertarsuaq.

The island is separated from Nuussuaq Peninsula in the northeast by the Sullorsuaq Strait. To the south of the island lies Disko Bay, an inlet bay of Baffin Bay. [2]

History

Research indicates that nine large tsunamigenic landslides struck Sullorsuaq Strait in prehistoric times during the Holocene, seven of them from the southern coast of the Nuussuaq Peninsula and two others from the northern coast of Disko Island. Seven of the landslides apparently occurred between about 8020 BC and 6520 BC with unidentified tsunamigenic effects. The two most recent prehistoric landslides generated megatsunamis which struck Alluttoq Island, the first sometime around 5650 BC with a run-up height of 41 to 66 metres (135 to 217 ft), and another that struck around 5350 BC with a run-up height of 45 to 70 metres (148 to 230 ft). [3]

Erik the Red paid the first recorded visit to Disko Island at some time between 982 and 985. The island was used as a base for summer hunting and fishing by Norse colonists. [4]

The coal mining town of Qullissat was founded on the northeast coast of Disko Island in 1924. [5] By 1952 it was a cultural hub and the third-largest settlement in Greenland, with a population of 995. [6] On 15 December 1952, a major landslide on a slope of the mountain Niiortuut ( 70°20′56″N53°10′41″W / 70.349°N 053.178°W / 70.349; -053.178 (Niiortuut) ) on the southern coast of the Nuussuaq Peninsula generated a tsunami which traveled 30 kilometres (19 mi) across Sullorsuaq Strait and struck Qullissat, where it had a run-up height of 2.2 to 2.7 metres (7 ft 3 in to 8 ft 10 in) and inflicted damage on buildings. [6] By 1966, Qullissat was the sixth-largest town in Greenland with a population of 1,400, [5] but it was abandoned in 1972, [7] leaving the northern coast of Disko Island uninhabited.

On 21 November 2000, a large landslide at Paatuut on the southern coast of the Nuussuaq Peninsula generated a megatsunami with a run-up height of 50 metres (164 ft) near the landslide and 28 metres (92 ft) at the former site of Qullissat, 20 kilometres (11 nmi; 12 mi) away, where it inundated the coast as far as 100 metres (328 ft) inland. [8]

Geology

Native iron from Disko Island (size: 4.9 x 2.9 x 1.5 cm [1.9 in. x1.1 in. x 0.6 in.]) Iron-sea07a.jpg
Native iron from Disko Island (size: 4.9 x 2.9 x 1.5 cm [1.9 in. x1.1 in. x 0.6 in.])
Polished slab from this same deposit, now at the Carnegie Museum of Natural History Native terrestrial iron from the Tertiary of Greenland.jpg
Polished slab from this same deposit, now at the Carnegie Museum of Natural History

Mineral deposits, fossil finds and geological formations add to interest in the area. One of the interesting geological features is the native iron found at the island. A 22-ton (44,000 lbs; 20 tonnes) lump mixture of iron and iron carbide (cohenite) has been found. There are only a few places on earth where native iron is found which is not of meteoric origin. [9] [10]

There are numerous hot springs on the island. The microscopic animal Limnognathia , the only known member of its phylum, was discovered in the Isunngua spring.

Biodiversity

Several studies on the meiofauna show high marine interstitial diversity in Disko Island. For instance, the gastrotrich species Diuronotus aspetos is found in Iterdla [11] and Kigdlugssaitsut [12] and is so far reported only in Disko Island. It is associated with a rich diversity of other gastrotrichs like Chaetonotus atrox , Halichaetonotus sp., Mesodasys sp., Paradasys sp., Tetranchyroderma sp., Thaumastoderma sp. and Turbanella sp. [11]

Related Research Articles

<span class="mw-page-title-main">Tsunami</span> Series of water waves caused by the displacement of a large volume of a body of water

A tsunami is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and underwater explosions above or below water all have the potential to generate a tsunami. Unlike normal ocean waves, which are generated by wind, or tides, which are in turn generated by the gravitational pull of the Moon and the Sun, a tsunami is generated by the displacement of water from a large event.

<span class="mw-page-title-main">Megatsunami</span> Very large wave created by a large, sudden displacement of material into a body of water

A megatsunami is a very large wave created by a large, sudden displacement of material into a body of water.

<span class="mw-page-title-main">Disko Bay</span> Bay on the western coast of Greenland

Disko Bay is a large bay on the western coast of Greenland. The bay constitutes a wide southeastern inlet of Baffin Bay.

<span class="mw-page-title-main">Pingo</span> Mound of earth-covered ice

Pingos are intrapermafrost ice-cored hills, 3–70 m (10–230 ft) high and 30–1,000 m (98–3,281 ft) in diameter. They are typically conical in shape and grow and persist only in permafrost environments, such as the Arctic and subarctic. A pingo is a periglacial landform, which is defined as a non-glacial landform or process linked to colder climates. It is estimated that there are more than 11,000 pingos on Earth, with the Tuktoyaktuk peninsula area having the greatest concentration at a total of 1,350. There is currently limited data on pingos.

Saqqaq is a settlement in the Avannaata municipality in western Greenland. Founded in 1755 as Solsiden, Saqqaq had 132 inhabitants in 2020. The village's Kalaallisut name is a translation of the Danish meaning "Sunny Side", in reference to its position relative to Livets Top.

Illorsuit is a former settlement in Avannaata municipality, in western Greenland. Located on the northeastern shore of Illorsuit Island − northwest of Uummannaq at the mouth of the Uummannaq Fjord − the settlement had 91 inhabitants in 2010. It was abandoned in 2018.

<span class="mw-page-title-main">Nuugaatsiaq</span> Place in Greenland, Kingdom of Denmark

Nuugaatsiaq is a settlement in the Avannaata municipality, in northwestern Greenland, located on an island off the southern coast of Sigguup Nunaa peninsula, in the Uummannaq Fjord basin. It had 84 inhabitants in 2010, but was abandoned after a tsunami struck in 2017.

<span class="mw-page-title-main">Alluttoq Island</span> Island in Greenland

Alluttoq Island is a large 655 km2 (252.9 sq mi), uninhabited island in Avannaata municipality in western Greenland, located in the northern part of Disko Bay, in the outlet of the Sullorsuaq Strait, east of Disko Island.

<span class="mw-page-title-main">Ella Island</span> Island in Greenland

Ella Island is an island in eastern Greenland, within Northeast Greenland National Park. It was established in 1941 to enforce Danish sovereignty in Greenland.. It is home of the legendary Sirius Dog Sled Patrol.

<span class="mw-page-title-main">Nuussuaq Peninsula</span> Peninsula in western Greenland

Nuussuaq Peninsula is a large peninsula in western Greenland.

<span class="mw-page-title-main">Qullissat</span> Place in Greenland, Kingdom of Denmark

Qullissat is a former settlement in the Qeqertalik municipality, located on the northeast coast of Disko Island on the west coast of Greenland. It was a coal mining town founded to exploit the natural resources of Disko Island. The mines operated for 48 years until 1972, when the economic base of the settlement collapsed, leading to its abandonment.

Sullorsuaq Strait is a strait on the western coast of Greenland.

Upernavik Archipelago is a vast coastal archipelago in the Avannaata municipality in northwestern Greenland, off the shores of northeastern Baffin Bay. The archipelago extends from the northwestern coast of Sigguup Nunaa peninsula in the south at approximately 71°50′N56°00′W to the southern end of Melville Bay in the north at approximately 74°50′N57°30′W.

<i>Diuronotus aspetos</i> Species of microscopic worm

Diuronotus aspetos is a species of large sized meiofaunal chaetonotid gastrotrich found in the North Atlantic. With Diuronotus rupperti, it is one of the only two species representing the genus Diuronotus.

Karrat Fjord is a fjord in Avannaata municipality in western Greenland.

<span class="mw-page-title-main">Cumbre Vieja tsunami hazard</span> Potential natural disaster

The island of La Palma in the Canary Islands is at risk of undergoing a large landslide, which could cause a tsunami in the Atlantic Ocean. Volcanic islands and volcanoes on land frequently undergo large landslides/collapses, which have been documented in Hawaii for example. A recent example is Anak Krakatau, which collapsed to cause the 2018 Sunda Strait tsunami.

The 1674 Ambon earthquake occurred on February 17 between 19:30 and 20:00 local time in the Maluku Islands. The resulting tsunami reached heights of up to 100 metres (330 ft) on Ambon Island killing over 2,000 individuals. It was the first detailed documentation of a tsunami in Indonesia and the largest ever recorded in the country. The exact fault which produced the earthquake has never been determined, but geologists postulate either a local fault, or a larger thrust fault offshore. The extreme tsunami was likely the result of a submarine landslide.

<span class="mw-page-title-main">1741 eruption of Oshima–Ōshima and the Kampo tsunami</span> Volcanic eruption and tsunami off the coast of Hokkaido

The devastating eruption of Oshima–Ōshima began on 18 August 1741 and ended on 1 May the next year. Eleven days into the eruption, the Kampo tsunami with estimated maximum heights of over 90 m (300 ft) swept across neighboring islands in Japan and the Korean Peninsula. The eruption and its resulting tsunami killed at least 1,400 people. Damage was extreme along the coast of Japan, while in Korea, the tsunami damaged fishing boats.

On September 16, 2023, a massive landslide occurred in Dickson Fjord, northeastern Greenland. It was triggered by a series of factors. Greenland, being highly sensitive to rising temperatures, has experienced accelerated glacial retreat and destabilization in recent years, making landslides more frequent and severe.

References

  1. Norwegian University of Science and Technology Archived 2011-06-15 at the Wayback Machine
  2. Nuussuaq, Saga Map, Tage Schjøtt, 1992
  3. Korsgaard, Niels J.; Svennevig, Kristian; Søndergaard, Anne S.; Luetzenburg, Gregor; Oksman, Mimmi; Larsen, Nicolaj K. (5 March 2024). "Evidence of Middle Holocene landslide-generated tsunamis recorded in lake sediments from Saqqaq, West Greenland". Natural Hazards and Earth System Sciences. 24 (3): 757–772. Bibcode:2024NHESS..24..757K. doi: 10.5194/nhess-24-757-2024 .
  4. Seaver, Kirsten A. (1996). "Greenland and Vínland: North Atlantic Exploration Five Hundred Years Before the Cabot Voyages". The Frozen Echo. pp. 14–43. doi:10.1515/9781503615731-004. ISBN   978-1-5036-1573-1.
  5. 1 2 "Qullissat" Ilulissat Museum
  6. 1 2 Svennevig, Kristian; Keiding, Marie; Korsgaard, Niels Jákup; Lucas, Antoine; Owen, Matthew; Poulsen, Majken Djurhuus; Priebe, Janina; Sørensen, Erik Vest; Morino, Costanza (February 2023). "Uncovering a 70-year-old permafrost degradation induced disaster in the Arctic, the 1952 Niiortuut landslide-tsunami in central West Greenland". Science of the Total Environment. 859: 160110. Bibcode:2023ScTEn.85960110S. doi:10.1016/j.scitotenv.2022.160110.
  7. "Suluk 2010 No.1" (PDF). Air Greenland. Archived from the original (PDF) on 9 June 2010. Retrieved 15 July 2010.
  8. Dahl-Jensen, Trine; Larsen, Lotte; Pedersen, Stig; Pedersen, Jerrik; Jepsen, Hans; Pedersen, Gunver; Nielsen, Tove; Pedersen, Asger; Von Platen-Hallermund, Frants; Weng, Willy (2004). "Landslide and Tsunami 21 November 2000 in Paatuut, West Greenland". repec.org. Ideas. Retrieved 14 October 2023.
  9. Bird; John M.; Goodrich; Cyrena Anne; Weathers; Maura S. (1981). "Petrogenesis of Uivfaq iron, Disko Island, Greenland". Journal of Geophysical Research. 86 (B12): 11787–11805. Bibcode:1981JGR....8611787B. doi:10.1029/JB086iB12p11787.
  10. W. Klöck; H. Palme & H. J. Tobschall (1986). "Trace elements in natural metallic iron from Disko Island, Greenland". Contributions to Mineralogy and Petrology. 93 (3): 273–282. Bibcode:1986CoMP...93..273K. doi:10.1007/BF00389387.
  11. 1 2 Balsamo M; Guidi L; Ferraguti M; Pierboni L & Kristensen RM (2010). "Diuronotus aspetos (Gastrotricha): new morphological data and description of the spermatozoon". Helgoland Marine Research. 64 (1): 27–34. Bibcode:2010HMR....64...27B. doi: 10.1007/s10152-009-0163-x .
  12. Todaro MA; Balsamo M & Kristensen RM (2005). "A new genus of marine chaetonotids (Gastrotricha) with a description of two new species from Greenland and Denmark". Journal of the Marine Biological Association of the United Kingdom. 83 (6): 1391–1400. Bibcode:2005JMBUK..85.1391T. doi:10.1017/S0025315405012579.